Table 1.
Observed blackbody temperature required to match the spectral continuum at different epochs.
Time (days) | Telescope/Instrument | Tobs (K) | Ref. |
---|---|---|---|
0.48 | Magellan/LDSS | 11 000![]() |
(1) |
0.53 | Magellan/MagE | 9300 ± 300 | (1) |
0.92 | ANU/WiFeS | 6800 ± 200 | (2) |
1.17 | SALT/RSS | 6400 ± 110 | (3) |
1.43 | VLT/X-shooter | 5440 ± 60 | (4) |
1.45 | VLT/X-shooter | 5380 ± 60 | (5) |
1.47 | SOAR/GHTS | 5330 ± 60 | (6) |
2.42 | VLT/X-shooter | 3940 ± 50 | (7) |
3.41 | VLT/X-shooter | 3420 ± 40 | (4) |
4.40 | VLT/X-shooter | 3230 ± 40 | (7) |
5.40 | VLT/X-shooter | 3070 ± 40 | (4) |
Notes. At t ≲1 day, the blackbody peaks in the UV, while for every subsequent spectrum, both the Rayleigh-Jeans and Wien tails are constrained. In these subsequent spectra, dust extinction uncertainties contribute the dominant statistical uncertainty to the blackbody temperature. In Fig. 3, we show the best-fit blackbodies alongside the observed spectra.
(1) Shappee et al. (2017) – these values of Tobs remain unchanged as no spectral features have been noted in these epochs; (2) Andreoni et al. (2017) – as the ANU spectrum does not strongly constrain the continuum shape, we report Tobs for this epoch as constrained by preceding and subsequent photometry – which suggests cooling from 7600 to 6600 K between 0.7 and 1.0 days post-merger (see Drout et al. 2017; (3) Buckley et al. (2018); (4) Pian et al. (2017); (5) Sneppen et al. (2023a); (6) Nicholl et al. (2017) – which is contemporaneous with NIR spectra from Gemini/FLAMINGOS-2 (see Chornock et al. 2017); (7) Smartt et al. (2017).
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